31 results were found for 【77AGG.COM】kd slot trisula 88 bos01 633 slot dodo slot vio77 slot tyq.

Results:

• 21. Journal_of_Hydrology_Veijalainen_etal

  /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 22. 2010_003rs

  við strik sprungunnar í heild, en þó er hún samhangandi við botninn. Hestvatnssprungan er einnig nær lóðrétt og um 15,5 km löng og með strikstefnu N179°A. Hún er ólík Holtasprungunni að því leyti að hún dýpkar til suðurs, úr 6 í 9 km en jafnframt virðist hún mynduð úr tveimur mishallandi flötum. Rétt sunnan skjálftamiðjunnar er sprungan nær lóðrétt (88° halli) en norðan upptakanna hallar /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 23. CES_D2.4_task1

  /media/ces/CES_D2.4_task1.pdf

• 24. GA_2009_91A_4_Andreassen

  net balances are wellcorrelated and (obviously) best modelled as the sum of bw measured and bs modelled (bs-m2). Thebest obtained correlations of modelled bw (0.86), bs(0.87) and bn (0.94) for 1949–2006, show that themodel could explain 73, 76 and 88% of the variance over this period.From each year we also extracted the day with maximum bw (bwd) and minimum bs (bsd, mini-mum values as bs is negative /media/ces/GA_2009_91A_4_Andreassen.pdf

• 25. Lorenzoni_Pidgeon_2006

  ). The implications of the present analysis are twofold. Firstly, a risk commu- nication strategy based on providing scientifically sound information alone, even if tailored to individuals’ perceptions of the issue and geared towards correcting 88 I. LORENZONI AND N. F. PIDGEON misinformed opinions (Kempton, 1997), whilst clearly outlining feasible actions individuals can undertake /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 26. Reykholt-abstracts

  in July 2016 on a Delta II rocket from Vandenberg Air Force Base in California. ICESat-2 will carry the Advanced Topographic Laser Altimeter System (ATLAS) and collect data to a latitudinal limit of 88 degrees. In contrast to Geoscience Laser Altimeter System (GLAS) on ICESat, ATLAS employs a 6-beam micro-pulse laser photon-counting approach. It uses a high repetition rate (10 kHz; 70 cm /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 27. 2010_016

  the following five parameters were adjusted: (1) Storage coefficient of direct runoff kd; (2) storage coefficient of interflow ki; (3) drainage density d; (4) the fraction of surface runoff from snowmelt; and (5) the recession constant krec for the decreasing saturated hydraulic conductivity with increasing depth. For the groundwater flow, adjusted parameters (6–7) are the hydraulic conductivity in the X /media/ces/2010_016.pdf

• 28. VI_2020_004

  .................... 85 8 Figure 57 50% PM10 probability map for an eruption like 1362 at Öræfajökull ..................... 86 Figure 58 The probability of exceedance curve at key locations (Öræfajökull) ...................... 87 Figure 59 Tephra accumulation rate on the ground on 7 May 1982 (Öræfajökull) ................. 88 Figure 60 Tephra accumulation rate on the ground on 5 May 1981 (Öræfajökull /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 29. VI_2019_009

  /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 30. VI_Arsskyrsla_2018_vef

  /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf